Image from the Biodiversity Heritage Library.
Contributed by Smithsonian Institution Archives.
| www.biodiversitylibrary.org
Transcription
190.- A short distance south
of Calvert's house, a road
leads of eastward and
then southward through
the woods, east of the
creek. Near the house
of Doringa Surpass, the
Black Shale rests on
the Coniferous at 1170.
The Coniferous is 13 feet
thick. The upper 3½ ft
are dark brown, contain
many calcite masses
but few crabs. The
lower 6½ feet are a light
brown limestone with
few fossils, and few
large crinoid stems such
as are characteristic
of the Devonian base.
The Coniferous rests di-
rectly on the Madison. The
nodular layer is seen in
the main road at 1200.
The Black Shale is at
least 35 feet thick.
191.- A mile and a quarter S. of
Alexaton, the Black Shale
rests on the Coniferous at
1140. A short distance N.
The Coniferous rests directly
on the Selkir clay & madine.
133
193.- A mile and a quarter east
of the junction of Mill Creek
with Scrut Grass
Creek is the house of James
White's house, north of the
creek, within cast of this
house the Black Shale
rests on the Coniferous at
1135. The Coniferous is
13 feet thick. The upper
4 feet are dark brown.
Below is a heavy chert
layer - 3-4 inches thick.
The lower 9 feet of Con-
iferous contain round
masses of chert; the
Coniferous rests directly
on the Madison beds. The
fossiliferous lower silice
shale is seen farther down
the hill.
194.- From ½ to 3/4 mile east
of James White's house, on
the south side of the creek is
the house of Sanford C. M.
McCarty. It is 3¼ miles
to Wilt Shell's hrg. The
Black Shale rests on the
Coniferous at 1140.